関東・東海地方における地殻水平変動-7-算出された地殻歪の状況
スポンサーリンク
概要
- 論文の詳細を見る
The characteristics of earth strain in the KANTO-TOKAI district calculated from the displacement vector are summarized as follows:1) The elongation with almost NNW-SSE direction is quite remarkable during for the coseismic earth strain of the 1923 KANTO earthquake.2) The principal axis of the postseismic compression is quite reverse as compared with the coseimic one.3) The principal axes of compression during the interseismic period are directed toward NW-SE in the TOKAI district, NNW-SSE in the KANTO district, and N-S in the BOSO peninsula.4) The maximum shear strain rates during the interseismic period are 2×10<SUP>-7</SUP>/yr. in the TOKAI district and 4×10<SUP>-7</SUP>/yr. in the KANTO district. In the KANTO district the calculated strain rate will be affected by the after effect of the 1923 KANTO earthquake.
- 日本測地学会の論文
日本測地学会 | 論文
- 月衝突盆地補償メカニズムの比較研究
- 重力異常に基づく糸魚川 - 静岡構造線北部の構造解析
- 台湾・竹崎観測室で観測された非等方性潮汐歪
- 電波無反射室におけるGPS測量用アンテナの位相特性の測定(続報)
- 4way ドップラー計測のロック判定方法と軌道上での検証